通过随机采集重建高动态范围陆地波场

GEOPHYSICS Pub Date : 2024-07-14 DOI:10.1190/geo2023-0506.1
Iga Pawelec, Paul Sava
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引用次数: 0

摘要

压缩传感(Compressive sensing,CS)是香农常规采样的一种替代方法,它能从减少的测量中捕捉相似的信息。它依靠随机采样模式和稀疏数据表示来重建常规采样对象。压缩采集是地震采集的重要组成部分,可改善近地表测绘和陆地数据的噪声抑制。然而,近地表捕获了震源产生的大部分能量,导致数据含有丰富的高波数内容,振幅跨越几个数量级。在处理这种高动态范围的非稳态数据时,傅立叶域无法提供最佳的稀疏表示,而稀疏表示是成功应用 CS 的必要条件。相比之下,离散复小波变换可以定位高能量特征,具有良好的方向选择性,并且接近移位不变性。综合这些特性,复小波能以紧凑的形式表示细节丰富的波场。为了充分利用这些特性并实现良好的 CS 重建,我们开发了一种与尺度和方向相关的迭代软阈值方案 (IST),用于重建高动态范围波场。我们的方法几乎不需要参数化,易于实现,并且对重建波场采样网格和动态范围具有鲁棒性。我们对随机缺失迹线的不同波场进行了 IST 测试,并将数据重建与频谱投影梯度求解器和凸集投影进行了比较。我们通过直接比较完全采样波场和重建波场的傅立叶系数来量化重建结果。在计算质量指标之前,先取傅里叶系数的对数 10,这样做既不强调幅度匹配的重要性,又突出了傅里叶系数支持的准确性,这通常会转化为重建数据的良好结构保真度。我们发现,IST 在所有示例中的表现一致,在进行温和去噪的同时,还能产生良好的相位匹配。
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High dynamic range land wavefield reconstruction from randomized acquisition
Compressive sensing (CS) is an alternative to regular Shannon sampling that captures similar information from reduced measurements. It relies on randomized sampling patterns and a sparse data representation to reconstruct the regularly sampled object. CS is an important ingredient in afford- able seismic acquisition which can lead to improvements in the near surface mapping and in noise suppression for land data. However, the near surface traps the majority of the source-generated energy, resulting in data that are rich in high-wavenumber content and have amplitudes spanning several orders of magnitude. When dealing with such high dynamic range non-stationary data, the Fourier domain is not optimal for providing a sparse representation - a necessary condition for successful application of CS. In contrast, a discrete complex wavelet transform can localize high energy features, has good directional selectivity, and is near-shift invariant. Combined, these properties allow complex wavelets to represent detail-rich wavefields in a compact form. To leverage these features and achieve good CS reconstructions, we develop a scale- and orientation- dependent iterative soft thresholding scheme (IST) for reconstructing high dynamic range wavefields. Our approach requires little parametrization, is easy to implement, and robust to reconstructed wave- field sampling grid and dynamic range. We test IST on different wavefields with randomly missing traces, and compare the data reconstructions to the spectral projected gradient solver and projection onto convex sets. We quantify the reconstructions by a direct comparison of Fourier coefficients between fully sampled and reconstructed wavefields. Taking log10 of Fourier coefficients prior to computing the quality metric de-emphasizes the importance of magnitude match while highlighting Fourier coefficient support accuracy which usually translates into good structural fidelity of reconstructed data. We find that IST performs consistently among all examples, yielding a good phase match while performing gentle denoising.
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